Predicting atmospheric background number concentration of ice nucleating particles in the Arctic

Mixed-phase clouds (MPCs) can have a net warming or cooling radiative effect on climate influenced by the phase and concentration of cloud particles. They have received considerable attention due to high spatial coverage and occurrence frequency in the Arctic. To initiate ice formation in MPCs at tem...

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Main Authors: Li, Guangyu, Wieder, Jörg, Pasquier, Julie T., Henneberger, Jan, Kanji, Zamin A.
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/acp-2022-21
https://acp.copernicus.org/preprints/acp-2022-21/
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spelling ftcopernicus:oai:publications.copernicus.org:acpd100749 2023-05-15T14:42:02+02:00 Predicting atmospheric background number concentration of ice nucleating particles in the Arctic Li, Guangyu Wieder, Jörg Pasquier, Julie T. Henneberger, Jan Kanji, Zamin A. 2022-01-27 application/pdf https://doi.org/10.5194/acp-2022-21 https://acp.copernicus.org/preprints/acp-2022-21/ eng eng doi:10.5194/acp-2022-21 https://acp.copernicus.org/preprints/acp-2022-21/ eISSN: 1680-7324 Text 2022 ftcopernicus https://doi.org/10.5194/acp-2022-21 2022-01-31T17:22:16Z Mixed-phase clouds (MPCs) can have a net warming or cooling radiative effect on climate influenced by the phase and concentration of cloud particles. They have received considerable attention due to high spatial coverage and occurrence frequency in the Arctic. To initiate ice formation in MPCs at temperatures above −38 °C, ice nucleating particles (INPs) are required, which therefore have important implications on the radiative properties of MPCs by altering the ice to liquid ratio of hydrometeors. As a result, constraining ambient INP concentrations could promote accurate representation of cloud microphysical processes and reduce the uncertainties in estimating the cloud-phase-related climate feedback in climate models. Currently, INP parameterizations are lacking for remote Arctic environments. Here we present INP number concentrations and their variability measured in Ny-Ålesund (Svalbard) at temperatures between 0 and −30 °C. No distinguishable seasonal difference was observed from 12 weeks of field measurements in autumn 2019 and spring 2020. In addition, correlating INP concentrations to aerosol physical properties was not feasible. Therefore, we propose a lognormal-distribution-based parameterization to predict Arctic INP concentration solely as a function of temperature. In practice, the parameterized variables allow for a) the prediction of the most likely INP concentrations and; b) the retrieval of the governing distribution of INP concentrations at given temperatures in the Arctic. Text Arctic Ny Ålesund Ny-Ålesund Svalbard Copernicus Publications: E-Journals Arctic Ny-Ålesund Svalbard
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Mixed-phase clouds (MPCs) can have a net warming or cooling radiative effect on climate influenced by the phase and concentration of cloud particles. They have received considerable attention due to high spatial coverage and occurrence frequency in the Arctic. To initiate ice formation in MPCs at temperatures above −38 °C, ice nucleating particles (INPs) are required, which therefore have important implications on the radiative properties of MPCs by altering the ice to liquid ratio of hydrometeors. As a result, constraining ambient INP concentrations could promote accurate representation of cloud microphysical processes and reduce the uncertainties in estimating the cloud-phase-related climate feedback in climate models. Currently, INP parameterizations are lacking for remote Arctic environments. Here we present INP number concentrations and their variability measured in Ny-Ålesund (Svalbard) at temperatures between 0 and −30 °C. No distinguishable seasonal difference was observed from 12 weeks of field measurements in autumn 2019 and spring 2020. In addition, correlating INP concentrations to aerosol physical properties was not feasible. Therefore, we propose a lognormal-distribution-based parameterization to predict Arctic INP concentration solely as a function of temperature. In practice, the parameterized variables allow for a) the prediction of the most likely INP concentrations and; b) the retrieval of the governing distribution of INP concentrations at given temperatures in the Arctic.
format Text
author Li, Guangyu
Wieder, Jörg
Pasquier, Julie T.
Henneberger, Jan
Kanji, Zamin A.
spellingShingle Li, Guangyu
Wieder, Jörg
Pasquier, Julie T.
Henneberger, Jan
Kanji, Zamin A.
Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
author_facet Li, Guangyu
Wieder, Jörg
Pasquier, Julie T.
Henneberger, Jan
Kanji, Zamin A.
author_sort Li, Guangyu
title Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
title_short Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
title_full Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
title_fullStr Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
title_full_unstemmed Predicting atmospheric background number concentration of ice nucleating particles in the Arctic
title_sort predicting atmospheric background number concentration of ice nucleating particles in the arctic
publishDate 2022
url https://doi.org/10.5194/acp-2022-21
https://acp.copernicus.org/preprints/acp-2022-21/
geographic Arctic
Ny-Ålesund
Svalbard
geographic_facet Arctic
Ny-Ålesund
Svalbard
genre Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-2022-21
https://acp.copernicus.org/preprints/acp-2022-21/
op_doi https://doi.org/10.5194/acp-2022-21
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